Sentence examples for atmosphere coupling from inspiring English sources

From the results of the present study, we were unable to definitively determine the stratosphere-mesosphere-ionosphere transport processes responsible for the observed ionosphere-neutral atmosphere coupling.

Non-migrating diurnal tidal wind speeds larger than 30 m/s are observed thus emphasizing the important role of non-migrating tides in middle atmosphere coupling.

The reason for this contradiction is that the GITM only includes the tidal wind, but excludes the tidal neutral compositions in the coupling between the lower atmosphere and thermosphere, while the TIEGCM includes both disturbances in the lower and upper atmosphere coupling.

With the continuous measurements of atmospheric electrical parameters and geomagnetic field variations, there is scope for addressing the problems related to the modulation of GEC by the influence of magnetosphere-ionosphere-lower atmosphere coupling processes on the near-surface electrical parameters in the polar caps.

Therefore, these examinations indicate that the strong coherence between the density and Nino3 index is likely a true signature of the lower upper atmosphere coupling during ENSO periods.

The models were run using Landsat imagery collected during the Soil Moisture Atmosphere Coupling Experiment (SMACEX) in 2002 and model results were compared with observations from a network of flux towers deployed within the study area.

It was a privilege to return there as a consultant cardiologist in 1983 and experience that same family atmosphere coupled with high quality of care.

The strange atmosphere, coupled with the cruel behavior of Mr. Wallenius, who deliberately flings a snake into a pool of oil to die, upsets Cress too much, so she runs home before the evening is over.

Since that time, investigators have broadened the scope of their research significantly, studying, for example, the continual recycling of the Earth's constituent materials through agencies of the hydrosphere and atmosphere coupled with seafloor spreading, mountain building, and other processes involving the terrestrial crust.

This phenomena is variously referred to as either ENSO-modoki [8 10], warm-pool ENSO [11], or central-Pacific ENSO [12, 13], and features basin-wide and decadal-scale variability in an ocean and atmosphere coupled system.

This phenomena is variously referred to as either ENSO-modoki [ 8- 10], warm-pool ENSO [ 11], or central-Pacific ENSO [ 12, 13], and features basin-wide and decadal-scale variability in an ocean and atmosphere coupled system.